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在实验室条件下研究岩石的射气扩散及它的射气作用是一个复杂而长期的过程。因此,最近注意了直接在天然条件下利用射气浓度按深部分布的实际曲线来研究这些作用的可能性。射气测深曲线(或简称ЭЗ曲线)的实验——理论研究表明,曲线形状主要取决于氡气的扩散速度,氡源在所研究的岩石中的分布特点及其岩层的厚度和分界面(边界条件)的气体交换条件。上述的每一个因素都决定着ЭЗ曲线的特征,从而,可根据曲线的形状求出确定的参数值。
It is a complicated and long-term process to study the radiofrequency and its radioactivity in rock under laboratory conditions. Therefore, attention has recently been paid to the possibility of studying these effects by using the actual profile of deep gas distribution directly under natural conditions using the gas concentration. Experimental-theoretical studies of a gas sounding curve (or simply ЭЗ curve) show that the shape of the curve depends mainly on the rate of radon diffusion, the distribution of radon sources in the rock under study, and the thickness and interface of the rock Boundary conditions) gas exchange conditions. Each of the above factors determines the characteristics of the ЭЗ curve so that certain parameter values can be found from the shape of the curve.